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Shanglun Formation

Shanglun Fm


Period: 
Devonian

Age Interval: 
D13 (65a), Emsian (late Early Devonian)


Province: 
Guangxi

Type Locality and Naming

The type section is located at Shanglun Village, 10 km east of Miaohuang Town of Xiangzhou County, Guangxi. It was named by Liu Jinrong Zhile in 1978 and placed in the lower part of Yujiang Stage. Yu C.M. et al. assigned it as a member to the lower Ertang Fm.

Synonym: Shanglun Dolomite


Lithology and Thickness

Dolomite. The Shanglun Formation consists mainly of gray to dark-gray medium- to thick-bedded dolomite intercalated with a few clayey limestone beds. In the type area, the Formation is about 185 m thick.

[Figure - Outcrop of Shanglun Dolomite in the Shuanggui Village of Ertang Town.]


Lithology Pattern: 
Dolomite


Relationships and Distribution

Lower contact

The lower boundary is conformable contact with underlying Yujiang Fm at the appearance of dolostone.

Upper contact

It is conformably overlain by the Ertang Fm.

Regional extent

It is mainly distributed in the west side of Dayaoshan Mt. It is correlated with a partial Huangjingshan Fm Dolomite of Beiliu and Najiao Fm Dolomite of Liujing, Hengxian. The thickness decreases from south to north and dies out to the north of Dale.


GeoJSON

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Fossils

The Shanglun Formation has poor fossils. Some fragments of small sized spiriferids and corals have been found.


Age 

Emsian (late Early Devonian)

Age Span: 

    Beginning stage: 
Emsian

    Fraction up in beginning stage: 
0.6

    Beginning date (Ma): 
400.78

    Ending stage: 
Emsian

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
399.16

Depositional setting

It is interpreted as a restricted platform environment.


Depositional pattern:  


Additional Information


Compiler:  

Hongfei Hou